Abstract
Knowledge of spatial and temporal hydroclimatic differences is critical in understanding climatic mechanisms. Here we show striking hydroclimatic contrasts between northern and southern parts of the eastern margin of the Tibetan Plateau (ETP), and those between East Asian summer monsoon (EASM) and Indian summer monsoon (ISM) areas during the past ~2,000 years. During the Medieval Period, and the last 100 to 200 years, the southern ETP (S-ETP) area was generally dry (on average), while the northern ETP (N-ETP) area was wet. During the Little Ice Age (LIA), hydroclimate over S-ETP areas was wet, while that over N-ETP area was dry (on average). Such hydroclimatic contrasts can be broadly extended to ISM and EASM areas. We contend that changes in sea surface temperatures (SSTs) of the tropical Pacific Ocean could have played important roles in producing these hydroclimatic contrasts, by forcing the north-south movement of the Intertropical Convergence Zone (ITCZ) and intensification/slowdown of Walker circulation. The results of sensitivity experiments also support such a proposition.
Document Type
Article
Publication Date
9-9-2016
Digital Object Identifier (DOI)
https://doi.org/10.1038/srep33177
Funding Information
This work was funded by the National Natural Science Foundation of China (Nos 41473120 and 41672169) and the National Basic Research Program of China (No. 2013CB955903).
Repository Citation
Xu, Hai; Lan, Jianghu; Sheng, Enguo; Liu, Bin; Yu, Keke; Ye, Yuanda; Shi, Zhengguo; Cheng, Peng; Wang, Xulong; Zhou, Xinying; and Yeager, Kevin M., "Hydroclimatic Contrasts Over Asian Monsoon Areas and Linkages to Tropical Pacific SSTs" (2016). Earth and Environmental Sciences Faculty Publications. 5.
https://uknowledge.uky.edu/ees_facpub/5
Supplementary Information
Included in
Earth Sciences Commons, Environmental Sciences Commons, Oceanography and Atmospheric Sciences and Meteorology Commons
Notes/Citation Information
Published in Scientific Reports, v. 6, article no. 33177, p. 1-9.
© The Author(s) 2016
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